A deterministic model of the vertical component of sediment motion in a turbulent fluid
โ Scribed by John C. Ludwick; George W. Domurat
- Publisher
- Elsevier Science
- Year
- 1982
- Tongue
- English
- Weight
- 847 KB
- Volume
- 45
- Category
- Article
- ISSN
- 0025-3227
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๐ SIMILAR VOLUMES
In turbulent flow, the normal procedure has been to seek means u of the fluid velocity u rather than the velocity itself. If these means are defined by local spacial averaging with an averaging radius of โฆ the approach is known as large eddy ลฝ . simulation, and u denotes the eddies of size 0 โฆ and l
## Abstract Drag coefficients of aerodynamically smooth spheres having a density variation of from 0.252 to 1.91 g./cc. and a diameter variation from 1.56 to 3.21 mm. were obtained for acceleration rates varying from 103.5 ft./sec.^2^ to โ30 ft./sec.^2^ and for relative intensities of up to 45%. Th